Switching between seismic and seismo-acoustic harmonic tremor simulated in the laborator:Insights into the role of open degassing channels and magma viscosity
Switching between seismic and seismo-acoustic harmonic tremor simulated in the laborator:Insights into the role of open degassing channels and magma viscosity
复制标题
实验室模拟的地震和地震声谐波颤动之间的切换:深入了解开放脱气通道和岩浆粘度的作用
DOI:
10.1002/jgrb.50067
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发表时间:
2013
期刊:
影响因子:
--
通讯作者:
and J. Lees
中科院分区:
文献类型:
--
作者:
J. Lyons;M. Ichihara;A. Kurokawa;and J. Lees
Switching between seismic‐only harmonic tremor (SHT) and seismo‐acoustic harmonic tremor (SAHT) has been reported at few volcanoes worldwide, but its occurrence may indicate important changes in shallow conduit conditions. Switching was simulated in a laboratory experiment in which harmonic signals were produced with a flow‐driven valve and compressed air. The harmonic signals were passed through a tank of shear‐thinning viscoelastic fluid, and the resulting signals were recorded. At high fluid stiffness, a stable, open conduit was produced, and the harmonic signals generated within the experimental apparatus were efficiently transmitted into the atmosphere. At lower fluid stiffness, bubbling dominated the activity, stable pathways were not generated in the fluid, and HT was not recorded in the atmosphere. These results are compared to observations of switching at Fuego volcano, Guatemala. We conclude that at intermediate magma viscosities, the development of stable degassing pathways open to the atmosphere will allow HT generated in the conduit to be transmitted into the atmosphere. Further, subtle changes in magma properties and supply rate may control whether SHT or SAHT is recorded, providing information about the state of the shallow conduit and vent at active volcanoes.